Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments
Mediterranean-climate catchments are characterized by significant spatial and temporal hydrological variability caused by the interaction of natural as well human-induced abiotic and biotic factors. This study investigates the non-linearity of rainfall-runoff relationship at multiple temporal scales...
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doaj-5be984f32a5d40d2826c41a0a7281e752020-11-25T02:20:25ZengMDPI AGWater2073-44412020-01-0112129910.3390/w12010299w12010299Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate CatchmentsJosep Fortesa0Jérôme Latron1Julián García-Comendador2Miquel Tomàs-Burguera3Jaume Company4Aleix Calsamiglia5Joan Estrany6Mediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainInstitute of Environmental Assessment and Water Research (IDAEA), Spanish Research Council (CSIC), Jordi Girona 18, 08034 Barcelona, SpainMediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainEstación Experimental de Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), 50192 Zaragoza, SpainMediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainMediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainMediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainMediterranean-climate catchments are characterized by significant spatial and temporal hydrological variability caused by the interaction of natural as well human-induced abiotic and biotic factors. This study investigates the non-linearity of rainfall-runoff relationship at multiple temporal scales in representative small Mediterranean-climate catchments (i.e., <10 km<sup>2</sup>) to achieve a better understanding of their hydrological response. The rainfall-runoff relationship was evaluated in 43 catchments at annual and event—203 events in 12 of these 43 catchments—scales. A linear rainfall-runoff relationship was observed at an annual scale, with a higher scatter in pervious (R<sup>2</sup>: 0.47) than impervious catchments (R<sup>2</sup>: 0.82). Larger scattering was observed at the event scale, although pervious lithology and agricultural land use promoted significant rainfall-runoff linear relations in winter and spring. These relationships were particularly analysed during five hydrological years in the Es Fangar catchment (3.35 km<sup>2</sup>; Mallorca, Spain) as a temporal downscaling to assess the intra-annual variability, elucidating whether antecedent wetness conditions played a significant role in runoff generation. The assessment of rainfall-runoff relationships under contrasted lithology, land use and seasonality is a useful approach to improve the hydrological modelling of global change scenarios in small catchments where the linearity and non-linearity of the hydrological response—at multiple temporal scales—can inherently co-exist in Mediterranean-climate catchments.https://www.mdpi.com/2073-4441/12/1/299rainfall-runoffmultiple temporal scalesnon-linearitysmall catchmentsmediterranean |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Josep Fortesa Jérôme Latron Julián García-Comendador Miquel Tomàs-Burguera Jaume Company Aleix Calsamiglia Joan Estrany |
spellingShingle |
Josep Fortesa Jérôme Latron Julián García-Comendador Miquel Tomàs-Burguera Jaume Company Aleix Calsamiglia Joan Estrany Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments Water rainfall-runoff multiple temporal scales non-linearity small catchments mediterranean |
author_facet |
Josep Fortesa Jérôme Latron Julián García-Comendador Miquel Tomàs-Burguera Jaume Company Aleix Calsamiglia Joan Estrany |
author_sort |
Josep Fortesa |
title |
Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments |
title_short |
Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments |
title_full |
Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments |
title_fullStr |
Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments |
title_full_unstemmed |
Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments |
title_sort |
multiple temporal scales assessment in the hydrological response of small mediterranean-climate catchments |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2020-01-01 |
description |
Mediterranean-climate catchments are characterized by significant spatial and temporal hydrological variability caused by the interaction of natural as well human-induced abiotic and biotic factors. This study investigates the non-linearity of rainfall-runoff relationship at multiple temporal scales in representative small Mediterranean-climate catchments (i.e., <10 km<sup>2</sup>) to achieve a better understanding of their hydrological response. The rainfall-runoff relationship was evaluated in 43 catchments at annual and event—203 events in 12 of these 43 catchments—scales. A linear rainfall-runoff relationship was observed at an annual scale, with a higher scatter in pervious (R<sup>2</sup>: 0.47) than impervious catchments (R<sup>2</sup>: 0.82). Larger scattering was observed at the event scale, although pervious lithology and agricultural land use promoted significant rainfall-runoff linear relations in winter and spring. These relationships were particularly analysed during five hydrological years in the Es Fangar catchment (3.35 km<sup>2</sup>; Mallorca, Spain) as a temporal downscaling to assess the intra-annual variability, elucidating whether antecedent wetness conditions played a significant role in runoff generation. The assessment of rainfall-runoff relationships under contrasted lithology, land use and seasonality is a useful approach to improve the hydrological modelling of global change scenarios in small catchments where the linearity and non-linearity of the hydrological response—at multiple temporal scales—can inherently co-exist in Mediterranean-climate catchments. |
topic |
rainfall-runoff multiple temporal scales non-linearity small catchments mediterranean |
url |
https://www.mdpi.com/2073-4441/12/1/299 |
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